Rock Identifier
Amethyst (Geode) (Silicon Dioxide (SiO2) with iron impurities) — mineral
mineral

Amethyst (Geode)

Silicon Dioxide (SiO2) with iron impurities

Hardness: 7 on Mohs scale; Color: Purple, violet, to deep lavender; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Hardness
7 on Mohs scale
Color
Purple, violet, to deep lavender
Luster
Vitreous (glassy)
Identified More mineral

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Physical properties

Hardness: 7 on Mohs scale; Color: Purple, violet, to deep lavender; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Formation & geological history

Formed in hydrothermal veins or cavities (vugs) within igneous rocks, particularly basalt. The purple hue is caused by irradiation of trivalent iron (Fe3+) within the crystal lattice. Most major deposits date back to the Cretaceous period.

Uses & applications

Primary use is in jewelry (faceted or cabochon), ornamental decoration (geodes and cathedrals), and as a popular specimen for mineral collectors.

Geological facts

Until the 18th century, amethyst was included in the cardinal gemstones alongside diamond, ruby, emerald, and sapphire. Large deposits found in Brazil significantly lowered its market value, making it accessible to many collectors.

Field identification & locations

Identify in the field by its distinct purple color, hexagonal prismatic crystal points, and lack of cleavage. Common locations include the Rio Grande do Sul region of Brazil, Artigas in Uruguay, and Ontario, Canada.